Plasma Astrophysics Chapter 2: Single Particle Motion Yosuke Mizuno Institute of Astronomy National Tsing-Hua University

Embed Size (px)

Citation preview

  • Slide 1
  • Plasma Astrophysics Chapter 2: Single Particle Motion Yosuke Mizuno Institute of Astronomy National Tsing-Hua University
  • Slide 2
  • Single Particle Motion Particle Motion in uniform B-field Gyro-motion E x B drift Particle Motion in non-uniform B-field Gradient drift Curvature drift Adiabatic invariants
  • Slide 3
  • Equation of Motion In dense plasma, Coulomb forces couple with particles. So bulk motion is significant In rarefied plasma, charge particles does not interact with other particles significantly. So motion of each particles can be treated independently In general, equation of motion of particle with mass m under influence of Lorentz force is : E: electric field, B: magnetic field, q: particles charge, v: particles velocity Which is valid for non-relativistic motion (v
  • Uniform B-field: Gyration If motion is only subject to static and uniform B field, (E=0 ) Taking a dot product with v, RHS is zero as v B => Therefore, a static magnetic field cannot change the kinetic energy of a particle since force is always perpendicular to direction of motion (2.2)
  • Slide 5
  • Uniform B-field: Gyration (cont.) Decompose velocity into parallel and perpendicular components to B: Eq (2.2) => This equation can be split into two independent equations: These imply that B field has no effect on the motion along it. Only affects particle velocity perpendicular it =>
  • Slide 6
  • Uniform B-field: Cyclotron Frequency To examine the perpendicular motion, we consider B =(0, 0, B z ) Re-write eq (2.2) in each components: To determine the time variation of v x and v y we take derivative eq (2.3a) & eq (2.3b), Where is the gyrofrequency or cyclotron frequency (2.3a) (2.3b) (2.3c) (2.4a) (2.4b)
  • Slide 7
  • Uniform B-field: Cyclotron Frequency (cont.) Gyrofrequency or cyclotron frequency: Indicative of the field strength and the charge and mass of particles of plasma Does not depend on kinetic energy For electron, c is positive, electron rotates in the right-hand sense Plasma can have several cyclotron frequencies Figure from Schwartz et al., P.23
  • Slide 8
  • Uniform B-field: Larmor radius The v x B force is centripetal, so Particles with faster velocities or larger mass orbit larger radii For electron, the gyrofrequency can be written: Larmor radius or gyroradius where B is in units of Gauss
  • Slide 9
  • Uniform B-field: Guiding Center What is path of electrons? Solution of eqs (2.4a) & (2.4b) are harmonic: where is a constant speed in plane of perpendicular to B Integrating, we have Using Larmor radius (r L ), and taking a real part of above: These describe a circular orbit at a guiding center (x 0, y 0 ) (2.5a) (2.5b) (2.6)
  • Slide 10
  • Uniform B-field: Helical Motion In addition to this motion, there is a velocity v z along B which is not effected by B Combine with eq (2.6), this gives helical motion about a guiding center Guiding center moves linearly along z with constant velocity, v || Pitch angle of helix is defined as guiding center motion in uniform B-field (x 0, y 0 ) rgrg rLrL
  • Slide 11
  • Helical Motion: Magnetic Moment The charge circulates on the plane perpendicular to B with a uniform angular frequency c Charge passes through c /2 times per unit time This motion equivalent with a situation that an electric current I=q c /2 is flowing in a circular coil with radius r L It has Magnetic moment: Therefore,
  • Slide 12
  • Uniform E & B field: E x B drift When E is finite, motion will be sum of two motions: circular Larmor gyration + drift of the guiding center Choose E to lie in x-z plane, so E y =0. consider B=(0,0,B z ), Equation of motion is z-component of velocity is: This is a straight acceleration along B. The transverse components are:
  • Slide 13
  • Uniform E & B field: E x B drift (cont.) Differentiating with constant E, Using we can write this as In a form similar to Eq (2.5a) & (2.5b): Larmor motion is similar to case when E=0, but now there is super-imposed drift v g of the guiding center in y direction
  • Slide 14
  • Uniform E & B field: E x B drift (cont.) To obtain the general formula for v g, we solve equation of motion As mdv/dt gives a circular motion, already understand this effect, so set to zero Taking cross product with B, The transverse components of this equation are Where v E is the E x B drift velocity of the guiding center
  • Slide 15
  • Uniform E & B field: E x B drift (cont.) vEvE
  • Slide 16
  • External force drift E x B drift of guiding center is : which can be extended to a form for a general force F: Example: In a gravitational field, Similar to the drift v E, in that drift is perpendicular to both forces, but in this case particles with opposite charge drift in opposite direction. External-force drift
  • Slide 17
  • Drift in non-uniform field Uniform fields provide poor descriptions for many phenomena, such as planetary fields, coronal loops in the Sun, Tokamaks, which have spatially and temporally varying fields. Particle drifts in inhomogeneous fields are classified several way In this lecture, consider two drifts associated with spatially non- uniform B: gradient drift and curvature drift. (There are many other) In general, introducing inhomogeneity is too complicated to obtain exact solutions for guiding center drifts Therefore use orbit theory approximation: Within one Larmor orbit, B is approximately uniform, i.e., typical length-scale L over which B varies is L >> r L => gyro-orbit is nearly circle
  • Slide 18
  • Grad-B Drift Assumes lines of forces are straight, but their strength is increases in y-direction Gradient in |B| causes the Larmor radius (r A =mv/qB) to be larger at the bottom of the orbit than at the top, which leads to a drift Drift should be perpendicular to B and B Ions and electrons drift in opposite directions
  • Slide 19
  • Grad-B Drift (cont.) Consider spatially-varying magnetic field, B=(0,0,B z (y)), i,.e., B only has z-component and the strength of it varies with y. Assume that E=0, so equation of motion is F=q(v x B) Separating into components, The gradient of B z is => This means that the magnetic field strength can be expanded in a Taylor expansion for distances y < r L, (2.7a ) (2.7b ) (2.7c )
  • Slide 20
  • Grad-B Drift (cont.) Expanding B z to first order in Eqs (2.7a) & (2.7b ) : Particles in B-field traveling around a guiding center (0,0) with helical trajectory: The velocities can be written in a similar form: Substituting these into eq(2.8) gives: (2.8a ) (2.8b )
  • Slide 21
  • Grad-B Drift (cont.) Since we are only interested in the guiding center motion, we average force over a gyro-period. Therefore in x-direction: But and => In the y-direction: Where but (2.9a ) (2.9b )
  • Slide 22
  • Grad-B Drift (cont.) In general, drift of guiding center is Using Eq(2.9b): So positive charged particles drift in x direction and negative charged particles drift +x direction In 3D, the result can be generalized to: The \pm stands for sign of charge. The grad-B drift is in opposite direction for electrons and ions and causes a current transverse to B Grad-B drift
  • Slide 23
  • Grad-B Drift (cont.) Below are shown particle drifts due to a magnetic field gradient, where B(y) = zB z (y) Consider r L =mv/qB, local gyroradius is large where B is small and is small where B is large which gives to a drift
  • Slide 24
  • Curvature Drift When charged particles move along curved magnetic field lines, experience centrifugal force perpendicular to magnetic field lines Assume radius of curvature (R c ) is >> r L The outward centrifugal force is This can be directly inserted into general form for guiding-center drift => Drift is into or out of page depending on sign of q Curvature drift
  • Slide 25
  • Adiabatic invariance of magnetic moment Gyrating particle constitutes an electric current loop with a dipole moment: The dipole moment is conserved, i.e., is invariant. Called the first adiabatic invariant. = const even if B varies spatially or temporally. If B varies, then v perp varies to keep = const =>v || also changes. It gives rise to magnetic mirrorng. Seen in planetary magnetospheres, coronal loops etc.
  • Slide 26
  • Magnetic mirroring Consider B-field is in z-direction and whose magnitude varies in z- direction. If B-field is axisymmetric, B =0 and d/d =0 (r, , z) This has cylindrical symmetry, so write How does this configuration gives a force that can trap a charged particle? Can obtain B r from. In cylindrical coordinates: If is given at r=0 and does not change much with r, then (2.10 )
  • Slide 27
  • Magnetic mirroring (cont.) Now have B r in terms of B z, which use to find Lorentz force on particle. The components of Lorentz force are: As B =0, two terms vanish and terms (1) & (2) give Larmor gyration. Term (3) vanishes on the axis and cause a drift in radial direction. Term (4) is therefore the one of interest Substitute from eq (2. 10): (1) (2) (3) (4)
  • Slide 28
  • Magnetic mirroring (cont.) Averaging over one gyro-orbit, and putting & r = r L This is called the mirror force, where -/+ arises because particles of opposite charge orbit the field in opposite directions. Above is normally written: or where In 3D, this can be generalized to: where F || is the mirror force parallel to B and ds is a line element along B
  • Slide 29
  • Adiabatic invariants Symmetry principles: Periodic motion conserved quantity symmetry conserved law What if the motion is almost periodic? Hamiltonian formulation: q and p is canonical variables and motion almost periodical => Adiabatic invariant is a property of physical system that stays constant when changes occur slowly is constant, called adiabatic invariant
  • Slide 30
  • First adiabatic invariant As particle moves into regions of stronger or weaker B, Larmor radius changes, but remains invariant To prove this, consider component of equation of motion along B: Multiplying by v || : Then, The particle energy must be conserved: Using (2.11 )
  • Slide 31
  • First adiabatic invariant (cont.) Use eq(2.11), As B is not equal to 0, this implies that: That is = const in time (invariant) is known as the first adiabatic invariant of the particle orbit. As a particle moves from a weak-field to a strong-field region, it sees B increasing and therefore v perp must increase in order to keep constant. Since total energy must remain constant, v || must decrease. If B is high enough, v || essentially => 0 and particle is reflected back to weak-field
  • Slide 32
  • Consequence of invariant Consider B 0 & B 1 in the weak- and strong-field regions. Associated speeds are v 0 & v 1 The conservation of implies that So as B increases, the perpendicular component of particle velocity increases => particles move more and more perpendicular to B However, since E=0, the total particle energy cannot increase. Thus as v perp increases, v || must decrease. The particle slow down in its motion along the filed If field is strong enough, at some point the particle may have v || =0
  • Slide 33
  • Consequence of invariant cont. At B 1, v 1,|| =0, From conservation of energy: Using we can write But, where is the pitch angle Therefore Particle with smaller will mirror in regions of higher B. If is too small, B 1 >> B 0 and particle does not mirror B v || v v perp
  • Slide 34
  • Consequence of invariant cont.2 Mirror ratio is defined as The smallest of a confined particle is This defines region in velocity space in the shape of a cone, called the loss cone. If a particle is in a region between two high field. The particle may be reflected at one, travel towards the second, and also reflect there. Thus the particle motion is confined to a certain region of space, this process is known as magnetic trapping.
  • Slide 35
  • Other adiabatic invariants Second adiabatic invariant: longitudinal invariant of a trapped particle in the magnetic mirror This property is used in Fermi acceleration. Third adiabatic invariant: flux invariant, which means the magnetic flux through the guiding center orbit is conserved
  • Slide 36
  • Application for Astrophysics Particle trapping: due to magnetic mirroring in the Earths van Allen radiation belt and energetic electrons confined in solar coronal magnetic loops Particle transport of energetic particles (galactic cosmic-rays, solar energetic particles, ultra-relativistic particles from extragalactic sources): governed by variety of particle drifts Particle acceleration: due to electric fields in pulsar magnetosphere and solar flares. Magnetic mirroring due to either stochastic motion of high field regions, or systematic motion between converging mirrors in the vicinity of shock waves, leads to Fermi acceleration of particles Radiation: given by relativistic gyrating particles (synchrotron radiation) or accelerating particles (bremsstrahlung)
  • Slide 37
  • Summary of single particle motion Charged particle motion in B & E fields is very unique and has interesting physical properties Particle Motion in uniform B-field (no E-field) Gyration: gyro (cyclotron)-frequency, Larmor radius, guiding center Particle Motion in uniform E & B-fields E x B drift Particle Motion in non-uniform B-field Grad-B drift, Curvature drift magnetic mirroring Adiabatic invariants Magnetic moment